Rock Identifier
Red Quartzite / River Cobble (Quartzite (SiO2 with iron oxide impurities)) — metamorphic
metamorphic

Red Quartzite / River Cobble

Quartzite (SiO2 with iron oxide impurities)

Hardness: 7 (Mohs scale), Color: Pinkish-red to maroon with grey veining, Luster: Vitreous to dull, Crystal Structure: Hexagonal (microcrystalline), Cleavage: None (conchoidal fracture), Specific Gravity: 2.6-2.7

Identified More metamorphic

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Physical properties

Hardness: 7 (Mohs scale), Color: Pinkish-red to maroon with grey veining, Luster: Vitreous to dull, Crystal Structure: Hexagonal (microcrystalline), Cleavage: None (conchoidal fracture), Specific Gravity: 2.6-2.7

Formation & geological history

Formed through the metamorphism of quartz-rich sandstone under intense heat and pressure. This specific rounded specimen has been weathered and shaped by water transport (alluvial process) in a river or glacial environment over thousands of years.

Uses & applications

Used as decorative landscaping stone, crushed aggregate for road construction, and occasionally for lapidary work like tumbled stones or cabochons due to its durability.

Geological facts

Quartzite is so tough that it often outlasts the mountain ranges from which it originated. It is frequently more resistant to chemical weathering than the marble it can sometimes be confused with physically.

Field identification & locations

Identify in the field by its inability to be scratched by a steel knife and its grainy, sandpaper-like texture beneath a smooth water-worn surface. Commonly found in riverbeds and glacial tills globally. Collectors look for unique vein patterns or intense coloration.